湘西更新世哺乳动物化石痕迹考察研究

目的 考察湘西土家族苗族自治州古丈县断龙乡猛虎洞更新世哺乳动物群骨化石断裂痕迹的状态与原因,探索湘西地区古人类活动的遗迹.方法 观测哺乳动物群骨化石断裂痕迹剖面的形态结构,以区别食肉类动物群的咬痕与人类打造的印迹.结果 经40件东方剑齿象、中国犀、鹿等残骨化石标本断裂痕迹剖面的观测,发现有部分骨化石断裂剖面圆钝,似啮齿动物的咬痕,但大部分骨化石断端剖面呈锥形切削改造,有的双面削刮呈锐利器型,有的存在明显打击或铲刮的 “印记”,初步认为属早期人类制作骨器的遗迹.结论 结合地理环境和地学结构分析,猛虎洞可能属晚更新世(10～5)万年前旧石器人类穴居的营地或系同生代古脊椎动物的遗址.     

加大宣传力度开发智力资源

论述了宣传在图书馆工作中的重要性和特点,从4个方面提出了高校图书馆宣传工作的具体措施。     

浅谈高校图书馆对艺术专业学生的特色服务

阐述了高校图书馆应根据艺术类专业学生的特点,通过开设艺术阅览室、增加艺术类报刊文献的收藏比例、根据艺术专业特点进行文献检索与利用教学、利用网络为学生提供服务等手段和方法,有区别、有针对性地开展特色服务。     

图书馆环境与读者健康

阐述了图书馆环境对读者生理及心理健康方面的影响,指出构建和谐的绿色图书馆是一项长期的工作任务,需要人们转变思想观念,同时争取社会各界的积极支持和广泛参与。     

Structural,morphological, and optical properties of tin(Ⅳ) oxide nanoparticles synthesized using Camellia sinensis extract: a green approach

Tin oxide (SnO2) nanoparticles were cost-effectively synthesized using nontoxic chemicals and green tea (Camellia sinensis) extract via a green synthesis method.The structural properties of the obtained nanoparticles were studied using X-ray diffraction,which indicated that the crystallite size was less than 20 nm.The particle size and morphology of the nanoparticles were analyzed using scanning electron microscopy and transmission electron microscopy.The morphological analysis revealed agglomerated spherical nanoparticles with sizes varying from 5 to 30 nm.The optical properties of the nanoparticles' band gap were characterized using diffuse reflectance spectroscopy.The band gap was found to decrease with increasing annealing temperature.The O vacancy defects were analyzed using photoluminescence spectroscopy.The increase in the crystallite size,decreasing band gap,and the increasing intensities of the UV and visible emission peaks indicated that the green-synthesized SnO2 may play future important roles in catalysis and optoelectronic devices.     

交错群A5，A6及射影特殊线性群L2(7)的一种新刻画

【目的】群的阶及群的共轭类的个数对群的结构有重要影响,探讨用群G的阶以及共轭类的个数k(G)刻画交错群A5,A6及射影特殊线性群L2(7)。 【方法】利用有限群的共轭类的长与元素的中心化子的阶的关系及群的素图与群的结构的关系, 使用分类讨论法及有限群的同构的判别法。 【结果】由|G|= 60,k(G)=5证明了G~=A5。同样地,由|G|=168,k(G)=6证明了G~=L2(7),由|G|=360,k(G)=7证明了G~=A6。【结论】通过给定群的阶以及共轭类的个数可以刻画某些有限单群,但是是否能够通过群的阶以及共轭类的个数共同刻画的单群都满足一些特殊的性质仍是一个开放的问题。     

Structural,compositional and mineralogical characterization of carbonatitic copper sulfide: Run of mine,concentrate and tailings

The aim of this study was to determine the structural, compositional, and mineralogical composition of carbonatitic copper sulfide concentrator plant streams. Three samples, each from a different stream(run of mine(ROM), concentrate, and tailings) of a copper concentrator were characterized using various techniques, including stereomicroscopy, X-ray fluorescence, X-ray diffraction, Fourier transform infrared(FTIR) spectroscopy, scanning electron microscopy(SEM) in conjunction with energy-dispersive X-ray spectroscopy(EDS), and optical microscopy. The results reveal that each stream possesses its own unique compositional features. Carbonate minerals associated with calcite and dolomite, followed by quartz, remain the major minerals in both the ROM and tails streams. In the ROM stream, chalcopyrite appears to occur as veins within the carbonatite-hosting ore body. Mineral phase mutation was discovered in the tails stream because magnetite formerly identified in the ROM as the primary iron oxide had evolved into hematite. This metamorphosis was likely promoted by the concentration process. The concentration process was effective, upgrading the chalcopyrite content from 2 wt% in the ROM stream to 58 wt% in the concentrate stream; it was accompanied by bornite(4 wt%), anilite(3 wt%), and digenite(2.5 wt%). In addition, the concentrate stream exhibited properties distinctive from those of the other streams. The FTIR analysis showed the existence of a sulfide group related to the chalcopyrite mineral. Free chalcopyrite grains were observed in the concentrate by SEM analysis, and their mineral presence was supported by the EDS analysis results. All characterization techniques corresponded well with each other regarding the structure, chemistry, and composition of the samples.     

泥石流危险性动量分区方法与应用

运用泥石流运动数值模拟和GIS相结合的方法模拟泥石流出山口后的运动全过程, 求得泥石流流速和流深分布, 确定泥石流过程中泛滥范围内任一点的最大动量, 建立了泥石流危险性动量分区模型Z = Khv. 根据考察和实验资料对委内瑞拉首都加拉加斯的Chacaito沟百年一遇泥石流运动过程进行了模拟, 利用动量分区方法划分出泥石流危险区.     

人行自助交通信号系统硬件模型的设计与实现

针对行人过路不方便且造成交通堵塞这一问题,阐述了人行自助交通信号系统硬件模型的设计与实现.